2) reef-beach body
生物礁滩体
3) organic reef and bank facies
生物礁滩相
1.
The organic reef and bank facies, widely developed in Middle Ordovician Yijianfang Formation in Tahe oilfield , are characterized by point reefs and banks within the caronate platforms, and the reservoir spaces are mainly of microfissures and secondary dissolution pores.
塔河油田中奥陶统一间房组广泛发育的生物礁滩相具有台地内部的点礁、点滩性质,储层的储集空间主要是微裂缝一次生溶蚀孔隙。
4) organic reef-bank complex
生物礁、滩复合体
5) beach reef
滩礁
6) bank and reef sedimentary facies
礁滩
1.
At the west margin of Sichuan basin is developed an assemblage of bank and reef sedimentary facies in Upper Triassic Ma\'antang formation.
四川盆地西缘上三叠统马鞍塘组发育一套礁滩组合,部分推覆到地表,部分埋藏在地下。
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性质: 见有机体
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